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      Exploring gold mineralization in altered ultramafic rocks in south Abu Marawat, Eastern Desert, Egypt

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          Abstract

          Gold mining is an important strategic sector. The search for mineral reserves is moving deeper as more accessible shallow resources are discovered. Geophysical techniques are now being employed more frequently in mineral exploration because they are quick and can provide crucial subsurface information for discovering potential metal deposits, particularly in high-relief and inaccessible places. The potential for gold in a large-scale gold mining (LSGM) locality in the South Abu Marawat area is investigated using a geological field investigation that includes rock sampling, structural measurements, detailed petrography, reconnaissance geochemistry, and thin section analysis, integrated with various transformation filters of surface magnetic data (analytic signal, normalized source strength, tilt angle), contact occurrence density maps, and tomographic modelling for the subsurface magnetic susceptibilities. The benefits of remote sensing (RS) and its technology in mapping detailed rock differentiation, and characterizing physical objects on the land surface using various spatial, and spectral resolution datasets are integrated. Both aeromagnetic and measured land magnetic profiles are used to investigate the area’s present geological conditions and possible future mining localities. Results indicate that gold mineralization in the study area is linked to the altered ultramafic zones that are associated with faulting and shearing and characterized by a low magnetic susceptibility anomaly.

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          Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution☆

          Graphicalabstract Condensed timetable of major geologic events in the East African Orogen. Opening of the Mozambique Ocean and formation of rift basins in Zambia, Malawi, Mozambique and SW Madagascar was accompanied by emplacement of anorthosite melt in extending crust. A first phase of ocean closure and accretion of terranes defines the East African Orogeny. The second orogen phase, Kuungan Orogeny, mainly affected the southern parts of east Africa and Madagascar. Both shortening events were followed by extension phases that were accompanied by emplacement of late- to post-tectonic granitoids. EGCD: Eastern Granulite–Cabo Delgado Nappe Complex; Madag: Madagascar; Ub–Us: Usagaran/Ubendian Belts; WG: Western Granulite Belt; IB (Z–M): Irumide Belt of Zambia and Malawi; IB (M): Irumide Belt of Mozambique.
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            Continental lithosphere of the Arabian Plate: A geologic, petrologic, and geophysical synthesis

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              Late Cryogenian–Ediacaran history of the Arabian–Nubian Shield: A review of depositional, plutonic, structural, and tectonic events in the closing stages of the northern East African Orogen

                Author and article information

                Contributors
                maazeem03@nriag.sci.eg
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                5 May 2023
                5 May 2023
                2023
                : 13
                : 7293
                Affiliations
                [1 ]GRID grid.7776.1, ISNI 0000 0004 0639 9286, Faculty of Science, Geology Department, , Cairo University, ; Giza, Egypt
                [2 ]GRID grid.459886.e, Geomagnetism and Geoelectricity Department, , National Research Institute of Astronomy and Geophysics, ; Helwan, Egypt
                [3 ]GRID grid.7776.1, ISNI 0000 0004 0639 9286, Faculty of Science, Geophysics Department, , Cairo University, ; Giza, Egypt
                Author information
                http://orcid.org/0000-0002-3483-9184
                http://orcid.org/0000-0001-8514-9290
                http://orcid.org/0000-0001-5417-926X
                https://orcid.org/0000-0003-3517-285X
                http://orcid.org/0000-0001-7350-5091
                http://orcid.org/0000-0002-1589-003X
                https://orcid.org/0000-0002-6274-9362
                Article
                33947
                10.1038/s41598-023-33947-w
                10163254
                37147329
                14efc567-b338-4237-b069-40a755ba8a55
                © The Author(s) 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 6 January 2023
                : 21 April 2023
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/501100003009, Science and Technology Development Fund;
                Award ID: 26277
                Funded by: The National Research Institute of Astronomy and Geophysics (NRIAG)
                Categories
                Article
                Custom metadata
                © The Author(s) 2023

                Uncategorized
                environmental sciences,solid earth sciences
                Uncategorized
                environmental sciences, solid earth sciences

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